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A tighter constraint on Earth-system sensitivity from long-term temperature and carbon-cycle observations
Tony E Wong1, Ying Cui2, Dana L Royer3
1School of Mathematical Sciences, Rochester Institute of Technology, Rochester, NY, USA. aewsma@rit.edu.
Nature Communications
|May 27, 2021
Summary
Earth system sensitivity (ESS) estimates were refined using a Bayesian approach with deep-time climate data. This study provides a narrower ESS range, improving climate change understanding.
Area of Science:
- Paleoclimatology
- Climate modeling
- Geochemistry
Background:
- Earth system sensitivity (ESS) is crucial for understanding long-term climate responses to CO2 forcing.
- Current ESS estimates have significant uncertainties, limiting climate projections.
- Previous studies constraining ESS often used informal statistics or focused on limited paleo-data.
Purpose of the Study:
- To refine Earth system sensitivity (ESS) estimates by integrating deep-time CO2 and temperature data with a long-term carbon cycle model.
- To reduce uncertainties in ESS and improve the quantification of Earth's long-term climate response.
- To investigate the role of chemical weathering in climate dynamics over geological timescales.
Main Methods:
- Employed a Bayesian approach to fuse extensive paleo-CO2 and temperature records (last 420 million years) with a sophisticated long-term carbon cycle model.
- Utilized deep-time climate data spanning 420 million years to constrain model parameters.
- Assessed the impact of varying chemical weathering parameters, specifically reduced weatherable land area, on model-data agreement.
Main Results:
- Generated a refined median ESS estimate of 3.4 °C, with a narrower 5-95% confidence range of 2.6-4.7 °C compared to previous assessments.
- Demonstrated that reduced chemical weathering, linked to decreased weatherable land area, improves model agreement with Cretaceous temperature records.
- Identified specific mechanisms within chemical weathering as key targets for future research to further constrain ESS.
Conclusions:
- The Bayesian fusion of deep-time data and carbon cycle modeling significantly narrows ESS uncertainty.
- Chemical weathering processes, particularly those related to land area, play a critical role in long-term climate regulation and ESS.
- Further research into weathering mechanisms offers a promising pathway to enhance our fundamental understanding of Earth system properties and climate sensitivity.
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